Loher, Markus; Pape, Thomas; Marcon, Yann; Römer, Miriam; Wintersteller, Paul; Praeg, Daniel; Torres, Marta E; Sahling, Heiko; Bohrmann, Gerhard (2017): Chloride and sulfate pore water analysis of sediment core GeoB19245-1. PANGAEA, https://doi.org/10.1594/PANGAEA.883405, In supplement to: Loher, M et al. (2018): Mud extrusion and ring-fault gas seepage – upward branching fluid discharge at a deep-sea mud volcano. Scientific Reports, 8, 6275, https://doi.org/10.1038/s41598-018-24689-1
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Project(s):
Coverage:
Latitude: 38.607583 * Longitude: 17.187050
Date/Time Start: 2014-12-02T15:06:00 * Date/Time End: 2014-12-02T15:08:00
Minimum DEPTH, sediment/rock: 0.220 m * Maximum DEPTH, sediment/rock: 4.980 m
Event(s):
GeoB19245-1 (M112/2_1258-1) * Latitude: 38.607583 * Longitude: 17.187050 * Date/Time Start: 2014-12-02T15:06:00 * Date/Time End: 2014-12-02T15:08:00 * Elevation: -1496.0 m * Recovery: 515 * Location: Venere mud volcano * Campaign: M112/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (GC) * Comment: bubbles before recovery, no storage
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Site | Site | Loher, Markus | |||
2 | DEPTH, sediment/rock | Depth sed | m | Loher, Markus | Geocode | |
3 | Chloride | Cl- | mmol/l | Loher, Markus | ||
4 | Sulfate | [SO4]2- | mmol/l | Loher, Markus |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
36 data points
Data
1 Site | 2 Depth sed [m] | 3 Cl- [mmol/l] | 4 [SO4]2- [mmol/l] |
---|---|---|---|
Venere W summit | 0.220 | 274.8 | 7.70 |
Venere W summit | 0.700 | 130.5 | 0.40 |
Venere W summit | 0.890 | 137.6 | 0.60 |
Venere W summit | 1.070 | 130.0 | 0.30 |
Venere W summit | 1.270 | 133.7 | 0.40 |
Venere W summit | 1.470 | 132.7 | 0.30 |
Venere W summit | 1.970 | 127.9 | 0.10 |
Venere W summit | 2.600 | 149.8 | 1.00 |
Venere W summit | 3.250 | 138.5 | 0.50 |
Venere W summit | 3.950 | 125.7 | 0.00 |
Venere W summit | 4.470 | 128.8 | 0.00 |
Venere W summit | 4.980 | 125.4 | 0.00 |